Cr-rich Picroilmenite
A variety of Ilmenite
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Formula:
Fe2+TiO3
A variety of Ilmenite
A cromium- and magnesium-rich variety of ilmenite, containing up to 8.6% Cr2O3 and up to 17.0% MgO.
A cromium- and magnesium-rich variety of ilmenite, containing up to 8.6% Cr2O3 and up to 17.0% MgO.
Unique Identifiers
Mindat ID:
40513 (as Cr-rich Picroilmenite)
2013 (as Ilmenite)
2013 (as Ilmenite)
Long-form identifier:
mindat:1:1:40513:1 (as Cr-rich Picroilmenite)
mindat:1:1:2013:4 (as Ilmenite)
mindat:1:1:2013:4 (as Ilmenite)
GUID
(UUID V4):
(UUID V4):
2798c047-39d3-461c-9dfb-162425f545e1 (as Cr-rich Picroilmenite)
4645b737-b289-4ac6-8bec-a3531e773cc3 (as Ilmenite)
4645b737-b289-4ac6-8bec-a3531e773cc3 (as Ilmenite)
Chemistry of Cr-rich Picroilmenite
Mindat Formula:
Fe2+TiO3
Elements listed:
Other Information
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
Internet Links for Cr-rich Picroilmenite
mindat.org URL:
https://www.mindat.org/min-40513.html
Please feel free to link to this page.
Please feel free to link to this page.
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References for Cr-rich Picroilmenite
Localities for Cr-rich Picroilmenite
Locality List
- This locality has map coordinates listed.
- This locality has estimated coordinates.
ⓘ - Click for references and further information on this occurrence.
? - Indicates mineral may be doubtful at this locality.
- Good crystals or important locality for species.
- World class for species or very significant.
(TL) - Type Locality for a valid mineral species.
(FRL) - First Recorded Locality for everything else (eg varieties).
Struck out - Mineral was erroneously reported from this locality.
Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).
All localities listed without proper references should be considered as questionable.
All localities listed without proper references should be considered as questionable.
China | |
| Guangcheng Zhang et al. (1983) |
| Guangcheng Zhang et al. (1983) |
| Guangcheng Zhang et al. (1983) |